🌋VolcanoAtlas

Nevados de Chillán

Chile's Volcanic Ski Resort Complex

Elevation

3,180 m

Last Eruption

2022

Type

Stratovolcano (compound)

Country

Chile

Location

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Volcanic Hazards & Risk Assessment

Primary Hazards

  • Pyroclastic flows
  • Lava flows
  • Volcanic bombs and ballistics
  • Lahars and mudflows

Risk Level

Population at RiskModerate
Infrastructure RiskHigh
Aviation RiskSignificant

Geological Composition & Structure

Rock Types

Primary
Unknown
Silica Content
Varied composition

Tectonic Setting

Unknown
Intraplate setting with hotspot or regional volcanic activity.

Age & Formation

Epoch
Unknown
Evidence
Unknown

Eruption Statistics & Analysis

MetricValueGlobal RankingSignificance
Total Recorded EruptionsUnknownLowModerately active volcano
Maximum VEIVEI UnknownMinorLocal impact potential
Recent Activity4 years agoVery RecentCurrently active

Monitoring & Alert Status

Monitoring Networks

Global Volcanism Program
International eruption database

Current Status

Active
Recent volcanic activity detected. Continuous monitoring in place.

Other Volcanoes in Chile

Interesting Facts

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Nevados de Chillán has produced 32 eruptions over nearly 9,000 years, making it one of Chile's most active volcanic complexes.

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The active vent has migrated progressively along the NNW–SSE axis over time: from Volcán Viejo (17th–19th centuries) to Volcán Nuevo (1906–1945) to Volcán Arrau (1973–1986) to Nicanor crater (2016–2022).

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Volcán Nuevo grew as a lava dome over a continuous 39-year eruption from 1906 to 1945 — one of the longest sustained dome-building episodes recorded at any Andean volcano.

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A major ski resort operates on the volcano's NW flank, making it one of the only ski resorts in the world built on a volcano that erupted within the past five years.

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Three nested Pleistocene calderas beneath the current volcanic complex produced ignimbrite sheets that traveled more than 100 km into Chile's Central Depression.

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The Volcán Arrau dome complex grew from 1973 to 1986 on the SE flank of Volcán Nuevo, eventually exceeding Nuevo's height.

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The 2016–2022 eruption at Nicanor crater lasted approximately six years, with dome growth, pyroclastic flows, and intermittent ash emissions.

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The name Nevados de Chillán means ‘Snow-capped (peaks) of Chillán’ in Spanish, and ‘Chillán’ derives from Mapuche language.

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Seasonal snow and small glaciers on the volcanic summits create lahar hazards when eruptions trigger rapid melting.

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The thermal hot springs (Termas de Chillán) on the volcano's flanks have been used since pre-Columbian times by the Mapuche people.

Frequently Asked Questions

Is Nevados de Chillán an active volcano?
Yes, Nevados de Chillán is classified as an active volcano and is one of Chile's most active volcanic complexes. The most recent eruption occurred from 2016 to 2022 at the Nicanor crater, lasting approximately six years. With 32 recorded eruptions spanning nearly 9,000 years, the complex has been in a near-continuous state of volcanic activity for centuries, with the active vent migrating progressively along the volcanic chain. SERNAGEOMIN continuously monitors the complex.
When did Nevados de Chillán last erupt?
The most recent eruption at Nevados de Chillán occurred from January 2016 to 2022, a sustained six-year event at the Nicanor crater reaching VEI 2. Activity included Vulcanian explosions, dome growth, pyroclastic flows, and intermittent ash emissions. Prior to this, the complex had experienced uncertain eruptions in 2009 and confirmed activity in 2003. The volcano is currently in a period of reduced activity with ongoing fumarolic emissions.
Is the ski resort safe on an active volcano?
The Nevados de Chillán ski resort operates on the northwestern flank of the volcanic complex, and its safety depends on the current volcanic activity level. During the 2016–2022 eruption, the resort periodically adjusted operations based on SERNAGEOMIN hazard advisories. The Chilean geological survey maintains comprehensive monitoring, and alert levels are communicated to resort operators and the public. Visitors should check current volcanic alert levels before traveling. Certain eruption scenarios could directly threaten the resort area with ashfall, pyroclastic flows, or lahars.
What type of volcano is Nevados de Chillán?
Nevados de Chillán is a compound stratovolcano, meaning it consists of multiple overlapping volcanic cones and domes built up over time along a linear structural trend. The complex includes Cerro Blanco, Volcán Viejo, Volcán Nuevo, Volcán Arrau, and the Nicanor crater, each representing a different period of activity. The andesitic to basaltic-andesitic composition produces a range of eruption styles from dome growth to moderate explosive eruptions. The complex sits within three nested Pleistocene calderas.
How tall is Nevados de Chillán?
The highest point of the Nevados de Chillán complex reaches 3,180 m (10,433 ft) above sea level. Multiple summits across the volcanic chain exceed 3,000 m. For comparison, the nearby Llaima volcano stands at 3,125 m, while Villarrica reaches 2,847 m. The complex's snow-capped peaks give it the ‘nevados’ (snowy) designation and support the ski resort operations on its flanks.
Why does the active vent keep moving?
The progressive migration of active vents along the NNW–SSE axis of the Nevados de Chillán complex is driven by the evolution of the volcanic plumbing system along a structural lineament. As magma pathways become blocked by solidified lava domes or altered rock, the rising magma finds new pathways along the structural trend, opening vents at new locations. This has produced a sequential chain of volcanic centers: from Cerro Blanco and Volcán Viejo to Volcán Nuevo, Volcán Arrau, and most recently the Nicanor crater. This behavior is common at compound volcanic complexes worldwide.
Where is Nevados de Chillán located?
Nevados de Chillán is located in the Ñuble Region of south-central Chile, in the Andes Mountains near the border with Argentina, at coordinates 36.868°S, 71.378°W. The complex lies approximately 50 km southeast of the city of Chillán (population ~180,000). It is part of the Southern Andean Volcanic Zone, which extends from central Chile to Patagonia and hosts some of South America's most active volcanoes.